Abstract
The Compton profile of polycrystalline MgO has been measured with MoKα X-rays scattered through 121°. The results obtained were compared with the profiles based on a superposition of Mg2+ and O2− ions. For Mg2+, Hartree-Fock free-ion wave functions were used, and the outer electrons in O2− were described by four sets of theoretical wave functions. The experimental results were in good agreement with the profile calculated from crystalline-field wave functions of O2−, whereas the models of fictitiously stabilized O2− ions proved to contain too much low momentum.